Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6384934 | Estuarine, Coastal and Shelf Science | 2014 | 14 Pages |
Abstract
Model simulations and empirical results show the presence of a cyclonic gyre in the central part of the ria that results from the combined effect of the Eume and the Mandeo river flows. Results suggest that the residual circulation is positive independently of the local wind regime and strongly depressed in the areas where mussel cultivation rafts are concentrated (up to 15%) as a result of their drag effects.163
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Pedro Duarte, Xosé Antón Alvarez-Salgado, Maria José Fernández-Reiriz, Silvia Piedracoba, UxÃo Labarta,